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考虑通过有意使平流层脱水来获取气候效益。

Considering intentional stratospheric dehydration for climate benefits.

作者信息

Schwarz Joshua P, Gao Ru-Shan, Thornberry Troy D, Rollins Andrew W, Rosenlof Karen H, Portmann Robert W, Bui ThaoPaul, Jensen Eric J, Ray Eric A

机构信息

NOAA Chemical Sciences Laboratory, Boulder, CO, USA.

NASA Ames Research Center, Moffett Field, CA, USA.

出版信息

Sci Adv. 2024 Mar;10(9):eadk0593. doi: 10.1126/sciadv.adk0593. Epub 2024 Feb 28.

Abstract

We introduce a climate intervention strategy focused on decreasing water vapor (WV) concentrations near the tropopause and in the stratosphere to increase outbound longwave radiation. The mechanism is the targeted injection of ice-nucleating particles (INP) in air supersaturated with respect to ice at high altitudes in the tropical entryway to the stratosphere. Ice formation in this region is a critical control of stratospheric WV. Recent airborne in situ data indicate that targeting only a small fraction of air parcels in the region would be sufficient to achieve substantial removal of water. This "intentional stratospheric dehydration" (ISD) strategy would not counteract a large fraction of the forcing from carbon dioxide but may contribute to a portfolio of climate interventions by acting with different time and length scales of impact and risk than other interventions that are already under consideration. We outline the idea, its plausibility, technical hurdles, and side effects to be considered.

摘要

我们引入了一种气候干预策略,该策略专注于降低对流层顶附近和平流层中的水汽(WV)浓度,以增加向外的长波辐射。其机制是在热带平流层入口的高海拔地区,向相对于冰呈过饱和状态的空气中有针对性地注入冰核粒子(INP)。该区域的冰形成是平流层水汽的关键控制因素。最近的机载原位数据表明,仅针对该区域一小部分气团就足以实现大量的水汽去除。这种“有意平流层脱水”(ISD)策略不会抵消大部分来自二氧化碳的强迫作用,但可能通过与其他正在考虑的干预措施在不同的时间和影响及风险长度尺度上发挥作用,从而为一系列气候干预措施做出贡献。我们概述了这一想法、其合理性、技术障碍以及需要考虑的副作用。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/a609/11809656/01c95633aa64/sciadv.adk0593-f1.jpg

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